Loading…

Three-dimensional geoelectrical model of metallogenic zones in the Kuznetsk-Alatau folded area

The three-dimensional (3D) geoelectric model of the Kuznetsk-Alatau folded area is reconstructed by magnetotelluric inversion using 3D fitting. It is established that the zones of ore mineralization within the Batenevsky massif are confined to the subvertical faults characterized by the electric res...

Full description

Saved in:
Bibliographic Details
Published in:Izvestiya. Physics of the solid earth 2012-11, Vol.48 (11-12), p.877-897
Main Authors: Belyavskii, V. V., Goidina, A. G.
Format: Article
Language:English
Subjects:
Citations: Items that this one cites
Items that cite this one
Online Access:Get full text
Tags: Add Tag
No Tags, Be the first to tag this record!
cited_by cdi_FETCH-LOGICAL-a339t-2454789d891198ccc94cd771bdff996bd79d7ac713043c7173bf5475b71ec5cb3
cites cdi_FETCH-LOGICAL-a339t-2454789d891198ccc94cd771bdff996bd79d7ac713043c7173bf5475b71ec5cb3
container_end_page 897
container_issue 11-12
container_start_page 877
container_title Izvestiya. Physics of the solid earth
container_volume 48
creator Belyavskii, V. V.
Goidina, A. G.
description The three-dimensional (3D) geoelectric model of the Kuznetsk-Alatau folded area is reconstructed by magnetotelluric inversion using 3D fitting. It is established that the zones of ore mineralization within the Batenevsky massif are confined to the subvertical faults characterized by the electric resistivity of 100–300 Ω m. Blocks with ρ ≈ 10−100 Ω m are identified at a depth below 10 km in the western part of the model. The blocks are located close to the areas marked by the increased thermal flux, reduced seismic velocities, and elevated Moho boundary. This is probably associated with the presence of the rift zone in this area.
doi_str_mv 10.1134/S106935131211002X
format article
fullrecord <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_journals_1266518157</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>2857860831</sourcerecordid><originalsourceid>FETCH-LOGICAL-a339t-2454789d891198ccc94cd771bdff996bd79d7ac713043c7173bf5475b71ec5cb3</originalsourceid><addsrcrecordid>eNp1kM1OwzAQhCMEEqXwANwscQ544ziOj1XFn6jEgSJxInLsTZvixMVODvTpcVUOSIjT7mrmG2knSS6BXgOw_OYFaCEZBwYZAKXZ21EyAc55WnBaHMc9yuleP03OQthQmudMyknyvlx7xNS0Hfahdb2yZIUOLerBtzpenTNoiWtIh4Oy1q2wbzXZuR4DaXsyrJE8jbseh_CRzqwa1EgaZw0aojyq8-SkUTbgxc-cJq93t8v5Q7p4vn-czxapYkwOaZbzXJTSlBJAllprmWsjBNSmaaQsaiOkEUoLYDRncQhWN5HgtQDUXNdsmlwdcrfefY4YhmrjRh-_CRVkRcGhBC6iCw4u7V0IHptq69tO-a8KaLWvsfpTY2SyAxOit1-h_5X8L_QNiAh0qg</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>1266518157</pqid></control><display><type>article</type><title>Three-dimensional geoelectrical model of metallogenic zones in the Kuznetsk-Alatau folded area</title><source>Springer Link</source><creator>Belyavskii, V. V. ; Goidina, A. G.</creator><creatorcontrib>Belyavskii, V. V. ; Goidina, A. G.</creatorcontrib><description>The three-dimensional (3D) geoelectric model of the Kuznetsk-Alatau folded area is reconstructed by magnetotelluric inversion using 3D fitting. It is established that the zones of ore mineralization within the Batenevsky massif are confined to the subvertical faults characterized by the electric resistivity of 100–300 Ω m. Blocks with ρ ≈ 10−100 Ω m are identified at a depth below 10 km in the western part of the model. The blocks are located close to the areas marked by the increased thermal flux, reduced seismic velocities, and elevated Moho boundary. This is probably associated with the presence of the rift zone in this area.</description><identifier>ISSN: 1069-3513</identifier><identifier>EISSN: 1555-6506</identifier><identifier>DOI: 10.1134/S106935131211002X</identifier><language>eng</language><publisher>Dordrecht: SP MAIK Nauka/Interperiodica</publisher><subject>Earth and Environmental Science ; Earth science ; Earth Sciences ; Electromagnetics ; Fracture zones ; Geophysics/Geodesy ; Mineralization ; Three dimensional imaging</subject><ispartof>Izvestiya. Physics of the solid earth, 2012-11, Vol.48 (11-12), p.877-897</ispartof><rights>Pleiades Publishing, Ltd. 2012</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a339t-2454789d891198ccc94cd771bdff996bd79d7ac713043c7173bf5475b71ec5cb3</citedby><cites>FETCH-LOGICAL-a339t-2454789d891198ccc94cd771bdff996bd79d7ac713043c7173bf5475b71ec5cb3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,776,780,27903,27904</link.rule.ids></links><search><creatorcontrib>Belyavskii, V. V.</creatorcontrib><creatorcontrib>Goidina, A. G.</creatorcontrib><title>Three-dimensional geoelectrical model of metallogenic zones in the Kuznetsk-Alatau folded area</title><title>Izvestiya. Physics of the solid earth</title><addtitle>Izv., Phys. Solid Earth</addtitle><description>The three-dimensional (3D) geoelectric model of the Kuznetsk-Alatau folded area is reconstructed by magnetotelluric inversion using 3D fitting. It is established that the zones of ore mineralization within the Batenevsky massif are confined to the subvertical faults characterized by the electric resistivity of 100–300 Ω m. Blocks with ρ ≈ 10−100 Ω m are identified at a depth below 10 km in the western part of the model. The blocks are located close to the areas marked by the increased thermal flux, reduced seismic velocities, and elevated Moho boundary. This is probably associated with the presence of the rift zone in this area.</description><subject>Earth and Environmental Science</subject><subject>Earth science</subject><subject>Earth Sciences</subject><subject>Electromagnetics</subject><subject>Fracture zones</subject><subject>Geophysics/Geodesy</subject><subject>Mineralization</subject><subject>Three dimensional imaging</subject><issn>1069-3513</issn><issn>1555-6506</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2012</creationdate><recordtype>article</recordtype><recordid>eNp1kM1OwzAQhCMEEqXwANwscQ544ziOj1XFn6jEgSJxInLsTZvixMVODvTpcVUOSIjT7mrmG2knSS6BXgOw_OYFaCEZBwYZAKXZ21EyAc55WnBaHMc9yuleP03OQthQmudMyknyvlx7xNS0Hfahdb2yZIUOLerBtzpenTNoiWtIh4Oy1q2wbzXZuR4DaXsyrJE8jbseh_CRzqwa1EgaZw0aojyq8-SkUTbgxc-cJq93t8v5Q7p4vn-czxapYkwOaZbzXJTSlBJAllprmWsjBNSmaaQsaiOkEUoLYDRncQhWN5HgtQDUXNdsmlwdcrfefY4YhmrjRh-_CRVkRcGhBC6iCw4u7V0IHptq69tO-a8KaLWvsfpTY2SyAxOit1-h_5X8L_QNiAh0qg</recordid><startdate>20121101</startdate><enddate>20121101</enddate><creator>Belyavskii, V. V.</creator><creator>Goidina, A. G.</creator><general>SP MAIK Nauka/Interperiodica</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7TG</scope><scope>7XB</scope><scope>88I</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>ARAPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>FR3</scope><scope>GNUQQ</scope><scope>H8D</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KL.</scope><scope>KR7</scope><scope>L.G</scope><scope>L7M</scope><scope>M2P</scope><scope>P5Z</scope><scope>P62</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>Q9U</scope></search><sort><creationdate>20121101</creationdate><title>Three-dimensional geoelectrical model of metallogenic zones in the Kuznetsk-Alatau folded area</title><author>Belyavskii, V. V. ; Goidina, A. G.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a339t-2454789d891198ccc94cd771bdff996bd79d7ac713043c7173bf5475b71ec5cb3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2012</creationdate><topic>Earth and Environmental Science</topic><topic>Earth science</topic><topic>Earth Sciences</topic><topic>Electromagnetics</topic><topic>Fracture zones</topic><topic>Geophysics/Geodesy</topic><topic>Mineralization</topic><topic>Three dimensional imaging</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Belyavskii, V. V.</creatorcontrib><creatorcontrib>Goidina, A. G.</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Meteorological &amp; Geoastrophysical Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>Technology Research Database</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Technology Collection</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>ProQuest Central (Alumni)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central</collection><collection>Advanced Technologies &amp; Aerospace Database‎ (1962 - current)</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Technology Collection</collection><collection>ProQuest Natural Science Collection</collection><collection>Earth, Atmospheric &amp; Aquatic Science Collection</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>ProQuest Central Student</collection><collection>Aerospace Database</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy &amp; Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Meteorological &amp; Geoastrophysical Abstracts - Academic</collection><collection>Civil Engineering Abstracts</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) Professional</collection><collection>Advanced Technologies Database with Aerospace</collection><collection>ProQuest Science Journals</collection><collection>ProQuest advanced technologies &amp; aerospace journals</collection><collection>ProQuest Advanced Technologies &amp; Aerospace Collection</collection><collection>Earth, Atmospheric &amp; Aquatic Science Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>ProQuest Central Basic</collection><jtitle>Izvestiya. Physics of the solid earth</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Belyavskii, V. V.</au><au>Goidina, A. G.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Three-dimensional geoelectrical model of metallogenic zones in the Kuznetsk-Alatau folded area</atitle><jtitle>Izvestiya. Physics of the solid earth</jtitle><stitle>Izv., Phys. Solid Earth</stitle><date>2012-11-01</date><risdate>2012</risdate><volume>48</volume><issue>11-12</issue><spage>877</spage><epage>897</epage><pages>877-897</pages><issn>1069-3513</issn><eissn>1555-6506</eissn><abstract>The three-dimensional (3D) geoelectric model of the Kuznetsk-Alatau folded area is reconstructed by magnetotelluric inversion using 3D fitting. It is established that the zones of ore mineralization within the Batenevsky massif are confined to the subvertical faults characterized by the electric resistivity of 100–300 Ω m. Blocks with ρ ≈ 10−100 Ω m are identified at a depth below 10 km in the western part of the model. The blocks are located close to the areas marked by the increased thermal flux, reduced seismic velocities, and elevated Moho boundary. This is probably associated with the presence of the rift zone in this area.</abstract><cop>Dordrecht</cop><pub>SP MAIK Nauka/Interperiodica</pub><doi>10.1134/S106935131211002X</doi><tpages>21</tpages></addata></record>
fulltext fulltext
identifier ISSN: 1069-3513
ispartof Izvestiya. Physics of the solid earth, 2012-11, Vol.48 (11-12), p.877-897
issn 1069-3513
1555-6506
language eng
recordid cdi_proquest_journals_1266518157
source Springer Link
subjects Earth and Environmental Science
Earth science
Earth Sciences
Electromagnetics
Fracture zones
Geophysics/Geodesy
Mineralization
Three dimensional imaging
title Three-dimensional geoelectrical model of metallogenic zones in the Kuznetsk-Alatau folded area
url http://sfxeu10.hosted.exlibrisgroup.com/loughborough?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-22T19%3A46%3A22IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Three-dimensional%20geoelectrical%20model%20of%20metallogenic%20zones%20in%20the%20Kuznetsk-Alatau%20folded%20area&rft.jtitle=Izvestiya.%20Physics%20of%20the%20solid%20earth&rft.au=Belyavskii,%20V.%20V.&rft.date=2012-11-01&rft.volume=48&rft.issue=11-12&rft.spage=877&rft.epage=897&rft.pages=877-897&rft.issn=1069-3513&rft.eissn=1555-6506&rft_id=info:doi/10.1134/S106935131211002X&rft_dat=%3Cproquest_cross%3E2857860831%3C/proquest_cross%3E%3Cgrp_id%3Ecdi_FETCH-LOGICAL-a339t-2454789d891198ccc94cd771bdff996bd79d7ac713043c7173bf5475b71ec5cb3%3C/grp_id%3E%3Coa%3E%3C/oa%3E%3Curl%3E%3C/url%3E&rft_id=info:oai/&rft_pqid=1266518157&rft_id=info:pmid/&rfr_iscdi=true